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Interpreting this variation between bulk and matrix density in terms of fracture porosity along the seismically observed fault zones, we may suggest fracture porosity in the order of 10%.
The hot spring emanations and hot wells at Fang do not lie on an observed fault trace.
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Inter turn fault is the second most commonly observed faults in the motors and is considered the most severe.
From Fig. 5b, the relay R7 8 is observing fault point in Zone-2 instead of Zone-1.
After observing fault localization with reduced area overhead, we utilize the self-checking full adder in constructing a self-repairing adder.
While it is true that operators sometimes fail to observe faults or other important signals, a quantitative analysis of monitoring behaviour shows that not even optimal sampling can detect all abnormal events.
However, when LG fault occurred at 250 km from Bus B1, the relay RA has observed the fault in Zone-2, even though the fault is in Zone-1.
We also discuss the relationship between the fault rupture and observed near-fault ground motions.
They observed a fault parallel ϕ for a period of 9 to 12 months after the mainshock, and a fault oblique ϕ for a period of 33 to 45 months after the mainshock.
Pyrite and quartz was observed along fault surfaces.
This was observed as fault assisted closures on the time structure map of the horizon.
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